Challenge from the simple: Some caveats in linearization of the Boyle-van't Hoff and Arrhenius plots

被引:7
|
作者
Katkov, Igor I. [1 ]
机构
[1] CELLTRONIX, San Diego, CA USA
关键词
Osmotic modeling; Cell loading; Linearization; Boyle-van't Hoff; Arrhenius; Osmotically inactive volume; Activation energy; Water permeability; Hydraulic conductivity; Solute permeability; Solute mobility;
D O I
10.1016/j.cryobiol.2008.07.009
中图分类号
Q [生物科学];
学科分类号
07 ; 0710 ; 09 ;
摘要
Some aspects of proper linearization of the Boyle-van't Hoff (BVH) relationship for calculation of the osmotically inactive volume v(b), and Arrhenius plot (AP) for the activation energy Ea are discussed. It is shown that the commonly used determination of the slope and the intercept (v(b)), which are presumed to be independent from each other, is invalid if the initial intracellular molality m(0) is known. Instead, the linear regression with only one independent parameter (v(b)) or the Least Square Method (LSM) with v(b) as the only fitting LSM parameter must be applied. The slope can then be calculated from the BVH relationship as the function of v(b). In case of unknown m(0) (for example, if cells are preloaded with trehalose, or electroporation caused ion leakage, etc.), it is considered as the second independent statistical parameter to be found. In this (and only) scenario, all three methods give the same results for v(b) and m(0). AP can be linearized only for water hydraulic conductivity (LP) and solute mobility (c),) while water and solute permeabilities P-w equivalent to LpRT and P-s equivalent to omega sRT cannot be linearized because they have pre-exponential factor (RT) that depends on the temperature T. (C) 2008 Elsevier Inc. All rights reserved.
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页码:142 / 149
页数:8
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